“…Based on morphological, crystallographic, magnetic, and chemical evidence, criteria or approaches have been proposed for identifying magnetofossils from sediments or rocks (e.g., Amor et al, 2015; Arató et al, 2005; Chang et al, 2016; Egli, 2004; Egli et al, 2010; Gehring et al, 2011, 2013; Kind et al, 2011; Li et al, 2012; Moskowitz et al, 1993; Thomas‐Keprta et al, 2000; Weiss et al, 2004). Although widely used, some of these criteria or approaches need to be reassessed because the crystal morphologies and arrangements of magnetosomal magnetic particles within modern MTB are diverse (e.g., Li, Benzerara, et al, 2013; Li, Menguy, et al, 2020; Liu et al, 2020; Pósfai et al, 2013), and spatial arrangements and/or chemical compositions of magnetofossils within the geological record may be altered during burial (e.g., Kopp & Kirschvink, 2008; Li et al, 2012; Li, Benzerara, et al, 2013; Roberts et al, 2013; Rodelli et al, 2019; Tarduno et al, 1998). Documenting bacterial diversity and biomineralization and magnetism of magnetosomal magnetic nanoparticles within modern MTB is, therefore, crucial for understanding the magnetofossil record.…”